{"pageNumber":"1919","pageRowStart":"47950","pageSize":"25","recordCount":68924,"records":[{"id":15053,"text":"ofr87203 - 1987 - Annual yield and selected hydrologic data for the Arkansas River Basin Compact, Arkansas-Oklahoma, 1986 water year","interactions":[],"lastModifiedDate":"2022-12-08T23:04:42.225901","indexId":"ofr87203","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1987","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":330,"text":"Open-File Report","code":"OFR","onlineIssn":"2331-1258","printIssn":"0196-1497","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"87-203","title":"Annual yield and selected hydrologic data for the Arkansas River Basin Compact, Arkansas-Oklahoma, 1986 water year","docAbstract":"<p>The computed annual yield and deficiency of the subbasins as defined in the Arkansas River Compact, Arkansas-Oklahoma, are given in tables. Actual runoff from the subbasins and depletion caused by major reservoirs in the compact area are also given in tabular form. Monthly, maximum, minimum, and mean discharges are shown for the 14 streamflow stations used in computing annual yield. Water quality data are shown for four sites in the compact area.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr87203","usgsCitation":"Moore, M.A., Lamb, T., and Blumer, S.P., 1987, Annual yield and selected hydrologic data for the Arkansas River Basin Compact, Arkansas-Oklahoma, 1986 water year: U.S. Geological Survey Open-File Report 87-203, iv, 38 p., https://doi.org/10.3133/ofr87203.","productDescription":"iv, 38 p.","costCenters":[],"links":[{"id":410200,"rank":3,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_17158.htm","linkFileType":{"id":5,"text":"html"}},{"id":43968,"rank":1,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1987/0203/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":147731,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1987/0203/report-thumb.jpg"}],"country":"United States","state":"Arkansas, Oklahoma","otherGeospatial":"Arkansas River Basin","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"coordinates\": [\n          [\n            [\n              -95.648,\n              36.425\n            ],\n            [\n              -95.648,\n              34.672\n            ],\n            [\n              -93.921,\n              34.672\n            ],\n            [\n              -93.921,\n              36.425\n            ],\n            [\n              -95.648,\n              36.425\n            ]\n          ]\n        ],\n        \"type\": \"Polygon\"\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ac8e4b07f02db67b7cd","contributors":{"authors":[{"text":"Moore, M. A.","contributorId":84767,"corporation":false,"usgs":true,"family":"Moore","given":"M.","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":170489,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Lamb, T.E.","contributorId":58272,"corporation":false,"usgs":true,"family":"Lamb","given":"T.E.","email":"","affiliations":[],"preferred":false,"id":170488,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Blumer, S. P.","contributorId":23938,"corporation":false,"usgs":true,"family":"Blumer","given":"S.","email":"","middleInitial":"P.","affiliations":[],"preferred":false,"id":170487,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":15063,"text":"ofr8728 - 1987 - Ground water-surface water relations in the Flathead River valley near the proposed Cabin Creek coal mine, British Columbia, Canada","interactions":[],"lastModifiedDate":"2012-02-02T00:07:03","indexId":"ofr8728","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1987","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":330,"text":"Open-File Report","code":"OFR","onlineIssn":"2331-1258","printIssn":"0196-1497","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"87-28","title":"Ground water-surface water relations in the Flathead River valley near the proposed Cabin Creek coal mine, British Columbia, Canada","docAbstract":"The area of the proposed Cabin Creek coal mine was studied to obtain information needed to respond to questions posed by the International Joint Commission advisers concerning water resources near the international border. Specific interest focused on determining the extent and character of surficial material in the Flathead River valley, identifying gaining and losing reaches of the river and major tributaries, and documenting ambient water quality at selected sites. Thickness of the alluvial deposits depends on depth to underlaying Quaternary glacial deposits or Tertiary bedrock. The alluvial deposits in the Flathead River valley thin to a veneer of cobbles near the mouth of Couldrey Creek. Measurements of streamflow at 20 sites in the Flathead River valley indicate that water discharges from the alluvial deposits to most of the tributaries and to the river near the proposed mine. The Flathead River gains 0.87 cu m/sec (31 cu ft/sec) of flow near Howell Creek. The Flathead River and Couldrey Creek gained about 0.81 cu m/sec (28.5 cu ft/sec) of flow near the mouth of Couldrey Creek where bedrock crops out in the streambeds. Bedrock outcrops effectively interrupt the alluvial aquifer system between the proposed mine site and the international border. The Flathead River lost 0.87 cu m/sec (31 cu ft/sec) of flow between the bedrock outcrops and the international border; this streamflow loss enters alluvial deposits and flows across the international border as subsurface flow. Analysis of samples from 18 stream sites and 1 spring site indicates general trends in water quality. In Howell Creek, concentrations of calcium, magnesium, and sulfates increased slightly downstream. Conversely, samples from Sage and Couldrey Creeks indicate downstream increases in concentrations of calcium, magnesium, and alkalinity, but decreases in concentrations of sulfate. Water quality of Cabin Creek was relatively stable through the sampled reach. Decreased concentrations of calcium and alkalinity in the Flathead River reflect the effect of inflow from Couldrey Creek and the groundwater inflow documented by streamflow measurements. (Author 's abstract)","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/ofr8728","usgsCitation":"Moreland, J.A., Liebscher, H., Van Voast, W., and Feltis, R., 1987, Ground water-surface water relations in the Flathead River valley near the proposed Cabin Creek coal mine, British Columbia, Canada: U.S. Geological Survey Open-File Report 87-28, iii, 20 p. :maps ;28 cm., https://doi.org/10.3133/ofr8728.","productDescription":"iii, 20 p. :maps ;28 cm.","costCenters":[],"links":[{"id":147630,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1987/0028/report-thumb.jpg"},{"id":43978,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1987/0028/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ab0e4b07f02db66d68d","contributors":{"authors":[{"text":"Moreland, J. A.","contributorId":71994,"corporation":false,"usgs":true,"family":"Moreland","given":"J.","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":170509,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Liebscher, Hugh","contributorId":25169,"corporation":false,"usgs":true,"family":"Liebscher","given":"Hugh","email":"","affiliations":[],"preferred":false,"id":170508,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Van Voast, W. A.","contributorId":16028,"corporation":false,"usgs":true,"family":"Van Voast","given":"W. A.","affiliations":[],"preferred":false,"id":170507,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Feltis, R.D.","contributorId":93467,"corporation":false,"usgs":true,"family":"Feltis","given":"R.D.","affiliations":[],"preferred":false,"id":170510,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}}
,{"id":15073,"text":"ofr86543 - 1987 - Estimation of the recharge area contributing water to a pumped well in a glacial-drift, river-valley aquifer","interactions":[{"subject":{"id":15073,"text":"ofr86543 - 1987 - Estimation of the recharge area contributing water to a pumped well in a glacial-drift, river-valley aquifer","indexId":"ofr86543","publicationYear":"1987","noYear":false,"title":"Estimation of the recharge area contributing water to a pumped well in a glacial-drift, river-valley aquifer"},"predicate":"SUPERSEDED_BY","object":{"id":2333,"text":"wsp2338 - 1989 - Estimation of the recharge area contributing water to a pumped well in a glacial-drift, river-valley aquifer","indexId":"wsp2338","publicationYear":"1989","noYear":false,"title":"Estimation of the recharge area contributing water to a pumped well in a glacial-drift, river-valley aquifer"},"id":1}],"supersededBy":{"id":2333,"text":"wsp2338 - 1989 - Estimation of the recharge area contributing water to a pumped well in a glacial-drift, river-valley aquifer","indexId":"wsp2338","publicationYear":"1989","noYear":false,"title":"Estimation of the recharge area contributing water to a pumped well in a glacial-drift, river-valley aquifer"},"lastModifiedDate":"2019-11-27T10:47:25","indexId":"ofr86543","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1987","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":330,"text":"Open-File Report","code":"OFR","onlineIssn":"2331-1258","printIssn":"0196-1497","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"86-543","title":"Estimation of the recharge area contributing water to a pumped well in a glacial-drift, river-valley aquifer","docAbstract":"The highly permeable, unconfined, glacial drift aquifers that occupy most New England river valleys constitute the principal source of drinking water for many communities that obtain part or all of their public water supply from groundwater. Analytical , two-dimensional numerical and three-dimensional numerical models were used to delineate contributing areas of groundwater pollution. These methods of analysis were compared by applying them to hypothetical aquifer having the dimensions and geometry of a typical glacial drift, river valley aquifer. In the model analyses, factors that control the size and shape of a contributing area were varied over ranges of values common to glacial drift aquifers in New England. These controlling factors include the rate of well discharge, rate of recharge to the aquifer from precipitation and from adjacent till and bedrock uplands, distance of a pumping well from a stream or other potential source of induced recharge, degree of hydraulic connection of the aquifer with a stream, horizontal hydraulic conductivity of the aquifer, ratio of horizontal to vertical hydraulic conductivity, and degree of well penetration. Numerical models of valley aquifers are deemed best suited to determine the approximate contributing area of a well because of their capability to simulate more accurately the variable geohydrologic conditions typical of glacial drift valley aquifers. On the basis of results obtained with the two-dimensional numerical model, for which a wide range of hydrologic conditions were simulated, the contributing area in a typical glacial drift, river valley setting for a well pumped at a rate of 1.0 million gal/day--a common pumping rate--can be expected to range from about 0.9 to 1.8 sq mi. Model analysis also shows that the contributing area of pumped wells may be expected to extend to the opposite side of the river and to include significant areas of till uplands adjacent to the aquifer on both sides of the valley. Simulations with the three-dimensional model allow a full delineation of the zone of contribution for a pumped well. For the relatively thin (100 ft or less) unconfined aquifers considered in this analysis, the model showed that the zone of contribution extended throughout the entire saturated thickness of aquifer. (Lantz-PTT)","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/ofr86543","usgsCitation":"Morrissey, D.J., 1987, Estimation of the recharge area contributing water to a pumped well in a glacial-drift, river-valley aquifer: U.S. Geological Survey Open-File Report 86-543, vi, 60 p. , https://doi.org/10.3133/ofr86543.","productDescription":"vi, 60 p. ","costCenters":[],"links":[{"id":369733,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1986/0543/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":148701,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1986/0543/report-thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a08e4b07f02db5fa4e5","contributors":{"authors":[{"text":"Morrissey, D. J.","contributorId":51305,"corporation":false,"usgs":true,"family":"Morrissey","given":"D.","email":"","middleInitial":"J.","affiliations":[],"preferred":false,"id":170524,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":49380,"text":"ofr87400C - 1987 - New information resources of the U.S. Geological Survey Library System, March 1987","interactions":[],"lastModifiedDate":"2012-02-02T00:11:21","indexId":"ofr87400C","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1987","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":330,"text":"Open-File Report","code":"OFR","onlineIssn":"2331-1258","printIssn":"0196-1497","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"87-400","chapter":"C","title":"New information resources of the U.S. Geological Survey Library System, March 1987","language":"ENGLISH","doi":"10.3133/ofr87400C","usgsCitation":"Water Resources Division, U.S. Geological Survey, 1987, New information resources of the U.S. Geological Survey Library System, March 1987: U.S. Geological Survey Open-File Report 87-400, 103 p., https://doi.org/10.3133/ofr87400C.","productDescription":"103 p.","costCenters":[],"links":[{"id":178722,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1987/0400c/report-thumb.jpg"},{"id":86024,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1987/0400c/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4afee4b07f02db697692","contributors":{"authors":[{"text":"Water Resources Division, U.S. Geological Survey","contributorId":128075,"corporation":true,"usgs":false,"organization":"Water Resources Division, U.S. Geological Survey","id":531900,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":17880,"text":"ofr86602 - 1987 - Water-resources activities of the U.S. Geological Survey in Texas— Fiscal years 1985–86","interactions":[],"lastModifiedDate":"2021-10-26T21:13:45.45852","indexId":"ofr86602","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1987","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":330,"text":"Open-File Report","code":"OFR","onlineIssn":"2331-1258","printIssn":"0196-1497","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"86-602","title":"Water-resources activities of the U.S. Geological Survey in Texas— Fiscal years 1985–86","docAbstract":"<p>Water-resources activities in Texas include collecting of hydrologic data, performing interpretive studies, and conducting research. This report describes the activities of the Water Resources Division of the U.S. Geological Survey in Texas for fiscal years (October to September) 1985 to 1986.</p>","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Austin, TX","doi":"10.3133/ofr86602","usgsCitation":"1987, Water-resources activities of the U.S. Geological Survey in Texas— Fiscal years 1985–86: U.S. Geological Survey Open-File Report 86-602, vii, 96 p., https://doi.org/10.3133/ofr86602.","productDescription":"vii, 96 p.","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":583,"text":"Texas Water Science Center","active":true,"usgs":true}],"links":[{"id":149810,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1986/0602/report-thumb.jpg"},{"id":390988,"rank":3,"type":{"id":36,"text":"NGMDB Index 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,{"id":13767,"text":"ofr87439 - 1987 - Publications of the U.S. Geological Survey Geothermal Research Program, 1982-1986","interactions":[],"lastModifiedDate":"2012-02-02T00:06:43","indexId":"ofr87439","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1987","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":330,"text":"Open-File Report","code":"OFR","onlineIssn":"2331-1258","printIssn":"0196-1497","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"87-439","title":"Publications of the U.S. Geological Survey Geothermal Research Program, 1982-1986","language":"ENGLISH","publisher":"The Survey,","doi":"10.3133/ofr87439","usgsCitation":"Water Resources Division, U.S. Geological Survey, 1987, Publications of the U.S. Geological Survey Geothermal Research Program, 1982-1986: U.S. Geological Survey Open-File Report 87-439, 38 p. ;28 cm., https://doi.org/10.3133/ofr87439.","productDescription":"38 p. ;28 cm.","costCenters":[],"links":[{"id":145345,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1987/0439/report-thumb.jpg"},{"id":42329,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1987/0439/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a90e4b07f02db655f9b","contributors":{"authors":[{"text":"Water Resources Division, U.S. Geological Survey","contributorId":128075,"corporation":true,"usgs":false,"organization":"Water Resources Division, U.S. Geological Survey","id":528964,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":14033,"text":"ofr87537 - 1987 - Water-quality data for Orwell reservoir and the Otter Tail River near Fergus Falls, Minnesota","interactions":[],"lastModifiedDate":"2018-03-12T11:52:45","indexId":"ofr87537","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1987","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":330,"text":"Open-File Report","code":"OFR","onlineIssn":"2331-1258","printIssn":"0196-1497","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"87-537","title":"Water-quality data for Orwell reservoir and the Otter Tail River near Fergus Falls, Minnesota","docAbstract":"<p>Water-quality data were collected at five sites on Orwell Reservoir and two sites on the Otter Tail River, at the inflow and outflow points of the reservoir. The data, collected from April 1983 to July 1966, consist mainly of streamflow and nutrient concentrations at the river sites and nutrient concentrations, alkalinity, Secchi-disk transparency, phytoplankton counts, chlorophyll concentrations, and profiles of specific conductance, temperature, pU, and dissolved oxygen at the reservoir sites. Additional data collected at the outflow site include alkalinity and concentrations of major ions and organic carbon.</p>","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"St. Paul, MN","doi":"10.3133/ofr87537","collaboration":"Prepared in cooperation with the U.S. Army Corps of Engineers","usgsCitation":"Have, M., and Tornes, L., 1987, Water-quality data for Orwell reservoir and the Otter Tail River near Fergus Falls, Minnesota: U.S. Geological Survey Open-File Report 87-537, v, 49 p., https://doi.org/10.3133/ofr87537.","productDescription":"v, 49 p.","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":392,"text":"Minnesota Water Science Center","active":true,"usgs":true}],"links":[{"id":42683,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1987/0537/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":147039,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1987/0537/report-thumb.jpg"}],"country":"United States","state":"Minnesota","county":"Otter Tail County","otherGeospatial":"Orwell Reservoir","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -96.191667,\n              46.233333\n            ],\n            [\n              -96.191667,\n              46.183333\n            ],\n            [\n              -96.108333,\n              46.183333\n            ],\n            [\n              -96.108333,\n              46.233333\n            ],\n            [\n              -96.191667,\n              46.233333\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a09e4b07f02db5fae16","contributors":{"authors":[{"text":"Have, M.R.","contributorId":79115,"corporation":false,"usgs":true,"family":"Have","given":"M.R.","affiliations":[],"preferred":false,"id":168823,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Tornes, L. H.","contributorId":103675,"corporation":false,"usgs":true,"family":"Tornes","given":"L. H.","affiliations":[],"preferred":false,"id":168824,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":14479,"text":"ofr87713 - 1987 - Arizona ground-water quality","interactions":[],"lastModifiedDate":"2012-02-02T00:07:04","indexId":"ofr87713","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1987","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":330,"text":"Open-File Report","code":"OFR","onlineIssn":"2331-1258","printIssn":"0196-1497","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"87-713","title":"Arizona ground-water quality","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/ofr87713","usgsCitation":"Kister, L., Radtke, D.B., and Graf, C., 1987, Arizona ground-water quality: U.S. Geological Survey Open-File Report 87-713, iv, 8 p. :ill., map ;28 cm., https://doi.org/10.3133/ofr87713.","productDescription":"iv, 8 p. :ill., map ;28 cm.","costCenters":[],"links":[{"id":148859,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1987/0713/report-thumb.jpg"},{"id":43173,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1987/0713/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4abce4b07f02db672ebb","contributors":{"authors":[{"text":"Kister, L. R.","contributorId":54187,"corporation":false,"usgs":true,"family":"Kister","given":"L. R.","affiliations":[],"preferred":false,"id":169523,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Radtke, D. B.","contributorId":72821,"corporation":false,"usgs":true,"family":"Radtke","given":"D.","email":"","middleInitial":"B.","affiliations":[],"preferred":false,"id":169524,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Graf, Charles","contributorId":6711,"corporation":false,"usgs":true,"family":"Graf","given":"Charles","email":"","affiliations":[],"preferred":false,"id":169522,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":18440,"text":"ofr88185 - 1987 - Water resources activities, Georgia district, 1987","interactions":[],"lastModifiedDate":"2019-11-27T10:04:05","indexId":"ofr88185","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1987","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":330,"text":"Open-File Report","code":"OFR","onlineIssn":"2331-1258","printIssn":"0196-1497","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"88-185","title":"Water resources activities, Georgia district, 1987","docAbstract":"<p>No abstract available.&nbsp;</p>","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/ofr88185","usgsCitation":"Casteel, C.A., and Ballew, M.D., 1987, Water resources activities, Georgia district, 1987: U.S. Geological Survey Open-File Report 88-185, iv, 62 p. , https://doi.org/10.3133/ofr88185.","productDescription":"iv, 62 p. 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,{"id":29336,"text":"wri854090 - 1987 - Hydrogeology of the surficial outwash aquifer at Cortland, Cortland County, New York","interactions":[],"lastModifiedDate":"2012-02-02T00:08:53","indexId":"wri854090","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1987","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":342,"text":"Water-Resources Investigations Report","code":"WRI","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"85-4090","title":"Hydrogeology of the surficial outwash aquifer at Cortland, Cortland County, New York","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/wri854090","usgsCitation":"Reynolds, R., 1987, Hydrogeology of the surficial outwash aquifer at Cortland, Cortland County, New York: U.S. Geological Survey Water-Resources Investigations Report 85-4090, v, 43 p. :ill., maps ;28 cm., https://doi.org/10.3133/wri854090.","productDescription":"v, 43 p. :ill., maps ;28 cm.","costCenters":[],"links":[{"id":119736,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1985/4090/report-thumb.jpg"},{"id":58177,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wri/1985/4090/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":58178,"rank":401,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wri/1985/4090/plate-2.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":58179,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1985/4090/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a2de4b07f02db614afb","contributors":{"authors":[{"text":"Reynolds, R.J.","contributorId":102921,"corporation":false,"usgs":true,"family":"Reynolds","given":"R.J.","email":"","affiliations":[],"preferred":false,"id":201365,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":2395,"text":"wsp2312 - 1987 - Geohydrology of the unsaturated zone at the burial site for low-level radioactive waste near Beatty, Nye County, Nevada","interactions":[{"subject":{"id":15210,"text":"ofr85198 - 1986 - Geohydrology of the unsaturated zone at the burial site for low-level radioactive waste near Beatty, Nye County, Nevada","indexId":"ofr85198","publicationYear":"1986","noYear":false,"title":"Geohydrology of the unsaturated zone at the burial site for low-level radioactive waste near Beatty, Nye County, Nevada"},"predicate":"SUPERSEDED_BY","object":{"id":2395,"text":"wsp2312 - 1987 - Geohydrology of the unsaturated zone at the burial site for low-level radioactive waste near Beatty, Nye County, Nevada","indexId":"wsp2312","publicationYear":"1987","noYear":false,"title":"Geohydrology of the unsaturated zone at the burial site for low-level radioactive waste near Beatty, Nye County, Nevada"},"id":1}],"lastModifiedDate":"2018-01-30T08:41:29","indexId":"wsp2312","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1987","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":341,"text":"Water Supply Paper","code":"WSP","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"2312","title":"Geohydrology of the unsaturated zone at the burial site for low-level radioactive waste near Beatty, Nye County, Nevada","docAbstract":"<p>Low-level radioactive solid waste has been buried in trenches at a site near Beatty, Nev., since 1962. In 1976, as part of a national program, the U.S. Geological Survey began a study of the geohydrology of the waste-burial site to provide a basis for estimating the potential for radionuclide migration in the unsaturated zone beneath the waste-burial trenches. Data collected include meteorological information for calibration of a long-term water-budget analysis, soil-moisture profiles, soil-water potentials, and hydraulic properties of representative unsaturated sediment samples to a depth of about 10 meters (m).</p><p>The waste-burial facility is in the northern Amargosa Desert about 170 kilometers (km) northwest of Las Vegas, Nevo The region is arid; mean annual precipitation at Lathrop Wells, 30 km south of the site, is only 7.4 centimeters (cm). The mean daily maximum temperature at Lathrop Wells in July, the hottest month, is 37 <span class=\"_Tgc _s8w\"><strong>°</strong></span><span class=\"_Tgc _s8w\"><strong></strong></span>C. The site is underlain by poorly stratified deposits of gravelly or silty sand and sandy gravel, and thick beds of clayey sediments. The total thickness of valley-fill deposits beneath the site is about 175 m; the unsaturated zone is about 85 m thick. Volumetric soil moisture to depths of 4 m ranges from 4 to 10 percent but commonly is in the range of 6 to 8 percent. Soil-water potential, measured to depths of 3 to 10 m, ranged from -10 to -70 bars. Unsaturated hydraulic conductivity computed from laboratory analyses of representative samples ranges from 10<sup>-13</sup> to 10<sup>-14</sup> centimeters per day (cm/d).</p><p>Evaporation studies over a 2-year (yr) period were used to calibrate a numerical procedure for analyzing long-term precipitation data and estimating annual water budgets during the 15-yr period 1962-76. This analysis (1) demonstrated that a potential exists for deep percolation (greater than 2 m), despite high annual evaporation demands, and (2) provided predictions of the time of year and the antecedent conditions that enhance the probability of deep percolation. Soil-moisture profiles obtained monthly over an 18-month (mo) period demonstrate that deep percolation does occur. Soil-moisture conditions antecedent to an observed deep-percolation event, and the time of year when the percolation occurred, support the interpretations based on long-term meteorological records.</p><p>Calculation of downward moisture movement through the waste-trench backfill material, on the basis of simplified assumptions, suggests that moisture could have penetrated as much as 6 m below land surface from 1963, when the oldest trenches were closed, to 1980, but that the moisture requirement for such penetration far exceeded the amount of moisture actually available. Steady-state downward movement of moisture at depths greater than 10 m and beneath the waste-burial trenches would be on the order of 4 cm per 1,000 yr, assuming a steady flux rate of 1x10<sup>-5</sup> cm/d.</p>","language":"English","publisher":"U.S. Government Printing Office","publisherLocation":"Washington, D.C.","doi":"10.3133/wsp2312","usgsCitation":"Nichols, W., 1987, Geohydrology of the unsaturated zone at the burial site for low-level radioactive waste near Beatty, Nye County, Nevada: U.S. Geological Survey Water Supply Paper 2312, Report: v, 57 p.; 1 Plate: 20.00 x 28.53 inches, https://doi.org/10.3133/wsp2312.","productDescription":"Report: v, 57 p.; 1 Plate: 20.00 x 28.53 inches","numberOfPages":"66","costCenters":[{"id":465,"text":"Nevada Water Science Center","active":true,"usgs":true}],"links":[{"id":139190,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wsp/2312/report-thumb.jpg"},{"id":28372,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/2312/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":28373,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wsp/2312/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"country":"United States","state":"Nevada","county":"Nye County","city":"Beatty","otherGeospatial":"Amargosa Desert","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b1ae4b07f02db6a87f7","contributors":{"authors":[{"text":"Nichols, William D.","contributorId":98296,"corporation":false,"usgs":true,"family":"Nichols","given":"William D.","affiliations":[],"preferred":false,"id":145131,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":25546,"text":"wri874115 - 1987 - Ground-water and soil contamination near two pesticide-burial sites in Minnesota","interactions":[],"lastModifiedDate":"2025-01-07T22:08:08.336463","indexId":"wri874115","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1987","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":342,"text":"Water-Resources Investigations Report","code":"WRI","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"87-4115","title":"Ground-water and soil contamination near two pesticide-burial sites in Minnesota","docAbstract":"<p>Preliminary investigations of the geology, groundwater hydrology , and soil and groundwater chemistry at sites in Pine and St. Louis Counties, Minnesota, have shown that contamination associated with pesticides buried at the sites is not widespread or highly concentrated. None of the pesticides sampled for in soil and in groundwater at the sites exceeded Minnesota soil and drinking water standards. About 1,500 pounds of lead arsenate were buried at the site in St. Louis County. Nearly 10,000 pounds of lead arsenate, as well as smaller quantities of organic pesticides (such as chlorpropham, DDT, endrin, and aldrin), lime sulfur, and magnesium carbonate were buried at the Pine County site. These chemicals were buried in shallow trenches at the sites during the early 1970's.</p>\n<p>The first wells drilled at each site were located to establish the direction of horizontal groundwater flow in each area. Groundwater flows to the northeast at the St. Louis County site and to the southeast at the Pine County site. Depths to the water table are about 30 ft at the Pine County site and about 25 ft at the St. Louis County site. In addition, groundwater is perched seasonally at about 5 ft below land surface in the immediate vicinity fo the burial site in Pine County. After the direction of flow was determined, additional wells were drilled down-gradient from the disposal areas at both sites to determine whether contaminations were migrating with groundwater away from the sites.</p>\n<p>In general, concentrations of lead and arsenic in soil and groundwater were below background concentrations for the areas. Concentrations of organic pesticides generally were below analytical-detection limits. The limited solubility of the chemicals and the tendency of the contaminants to be sorbed on soil particles probably combined to restrict mobilization of the chemicals.</p>","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"St. Paul, MN","doi":"10.3133/wri874115","collaboration":"Prepared in cooperation with the Minnesota Department of Natural Resources","usgsCitation":"Stark, J., Strudell, J., Bloomgren, P., and Eger, P., 1987, Ground-water and soil contamination near two pesticide-burial sites in Minnesota: U.S. Geological Survey Water-Resources Investigations Report 87-4115, vii, 48 p., https://doi.org/10.3133/wri874115.","productDescription":"vii, 48 p.","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":392,"text":"Minnesota Water Science 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J. R.","contributorId":100406,"corporation":false,"usgs":true,"family":"Stark","given":"J. R.","affiliations":[],"preferred":false,"id":194139,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Strudell, J.D.","contributorId":16869,"corporation":false,"usgs":true,"family":"Strudell","given":"J.D.","email":"","affiliations":[],"preferred":false,"id":194136,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Bloomgren, P.A.","contributorId":19599,"corporation":false,"usgs":true,"family":"Bloomgren","given":"P.A.","email":"","affiliations":[],"preferred":false,"id":194137,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Eger, P.","contributorId":26330,"corporation":false,"usgs":true,"family":"Eger","given":"P.","email":"","affiliations":[],"preferred":false,"id":194138,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}}
,{"id":13202,"text":"ofr84467 - 1987 - Hydrology of area 46, Northern Great Plains and Rocky Mountain coal provinces, North Dakota","interactions":[],"lastModifiedDate":"2018-02-16T14:15:25","indexId":"ofr84467","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1987","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":330,"text":"Open-File Report","code":"OFR","onlineIssn":"2331-1258","printIssn":"0196-1497","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"84-467","title":"Hydrology of area 46, Northern Great Plains and Rocky Mountain coal provinces, North Dakota","docAbstract":"<p>This report is one of a series that describes the hydrology of coal provinces nationwide. The Northern Great Plains and Rocky Mountain Coal Provinces are divided into 20 separate reporting areas which are numbered 43 to 62. This report provides general hydrologic information for Area 46 using a brief text with accompanying maps, charts, or graphs. This information may be used to describe the hydrology of the general area of any existing or proposed mine. Some of the more obvious hydrologic problems of coal development that will need to be addressed before development are disruption of aquifers and potential contamination of streams, aquifers, and the atmosphere.</p><p>Area 46 is in northwestern North Dakota and is composed of parts or all of 14 hydrologic units based on surface-water drainage basins. The area is drained by the Missouri and Souris Rivers.</p><p>Lignite-bearing rocks of late Paleocene age underlie nearly all of Area 46. The thickest and most continuous lignite beds occur in the Sentinel Butte and Tongue River Members of the Fort Union Formation. Alluvial deposits and a veneer of glacial drift of late Pleistocene age overlie the lignite-bearing rocks. </p><p>The climate of the area is semiarid. Mean annual precipitation ranges from 13.9 to 17.8 inches.&nbsp;Mean annual temperatures range from 37.7°F at Bowbells to 40.9°F at Williston. Mean monthly temperatures at Williston range from 8.3°F to 70°F. The growing season is about 125 days.</p><p>A fairly comprehensive data base for streamflow and water quality in streams is available for Area 46. Many of the small-stream monitoring sites have been operated during the last few years to provide a data base before coal development. With the exception of the Missouri River, which is controlled by several dams, both the quantity and quality of water varies greatly in all streams. </p><p>A ground-water observation network for water levels and water quality has been established through county ground-water resource investigations and other ground-water studies and provides an adequate data base. </p><p>Three activities within the U.S. Geological Survey identify and provide access to hydrologic data. These are the National Water-Data Exchange (NAWDEX), the National Water-Data Storage and Retrieval System (WATSTORE), and the Office of Water-Data Coordination (OWDC).</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr84467","usgsCitation":"Croft, M., and Crosby, O.A., 1987, Hydrology of area 46, Northern Great Plains and Rocky Mountain coal provinces, North Dakota: U.S. Geological Survey Open-File Report 84-467, v, 80 p., https://doi.org/10.3133/ofr84467.","productDescription":"v, 80 p.","numberOfPages":"88","costCenters":[{"id":478,"text":"North Dakota Water Science Center","active":true,"usgs":true},{"id":34685,"text":"Dakota Water Science Center","active":true,"usgs":true}],"links":[{"id":147314,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1984/0467/report-thumb.jpg"},{"id":95110,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1984/0467/report.pdf","size":"24089","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a13e4b07f02db601ff2","contributors":{"authors":[{"text":"Croft, M.G.","contributorId":55413,"corporation":false,"usgs":true,"family":"Croft","given":"M.G.","email":"","affiliations":[],"preferred":false,"id":167397,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Crosby, Orlo A.","contributorId":149073,"corporation":false,"usgs":false,"family":"Crosby","given":"Orlo","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":167398,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":55212,"text":"wdrIA861 - 1987 - Water resources data Iowa, water year 1986","interactions":[],"lastModifiedDate":"2016-03-07T14:24:40","indexId":"wdrIA861","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1987","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":340,"text":"Water Data Report","code":"WDR","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"IA-86-1","title":"Water resources data Iowa, water year 1986","docAbstract":"<p>Water resources data for the 1986 water year for Iowa consist of records of stage, discharge, and water quality of streams; stage, contents, and water quality of lakes and reservoirs; ground-water levels and ground-water quality. This report contains discharge records for 110 stream-gaging stations; stage and contents for 8 lakes and reservoirs; water quality for 8 stream-gaging stations; sediment records for 10 streamgaging stations; water levels for 108 observation wells; and chemical analyses for 214 observation wells. Also included are 116 crest-stage partial-record stations. Additional water data were collected at various sites, not part of the systematic data-collection program, and are published as miscellaneous measurements and analyses. The data represent that part of the National Data System operated:\"by the U.S. Geological Survey and cooperating State and Federal agencies in Iowa.</p>","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Iowa City","doi":"10.3133/wdrIA861","collaboration":"Prepared in cooperation with the Geological Survey Bureau, Iowa Department of Natural Resources, Iowa Department of Transportation and with Federal agencies","usgsCitation":"Melcher, N., Detroy, M., Matthes, W., and Karsten, R., 1987, Water resources data Iowa, water year 1986: U.S. Geological Survey Water Data Report IA-86-1, xv, 333 p., https://doi.org/10.3133/wdrIA861.","productDescription":"xv, 333 p.","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":351,"text":"Iowa Water Science 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,{"id":14949,"text":"ofr87735 - 1987 - Missouri ground-water quality","interactions":[],"lastModifiedDate":"2012-02-02T00:06:48","indexId":"ofr87735","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1987","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":330,"text":"Open-File Report","code":"OFR","onlineIssn":"2331-1258","printIssn":"0196-1497","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"87-735","title":"Missouri ground-water quality","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/ofr87735","usgsCitation":"Mesko, T.O., and Berkas, W., 1987, Missouri ground-water quality: U.S. Geological Survey Open-File Report 87-735, iv, 9 p. :ill., maps ;28 cm., https://doi.org/10.3133/ofr87735.","productDescription":"iv, 9 p. :ill., maps ;28 cm.","costCenters":[],"links":[{"id":145946,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1987/0735/report-thumb.jpg"},{"id":43765,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1987/0735/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b05e4b07f02db699acc","contributors":{"authors":[{"text":"Mesko, T. O.","contributorId":83934,"corporation":false,"usgs":true,"family":"Mesko","given":"T.","email":"","middleInitial":"O.","affiliations":[],"preferred":false,"id":170302,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Berkas, W.R.","contributorId":59808,"corporation":false,"usgs":true,"family":"Berkas","given":"W.R.","affiliations":[],"preferred":false,"id":170301,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":40036,"text":"ofr85648E - 1987 - Data on ground-water quality for the McDermitt 1° x 2° quadrangle, northern Nevada","interactions":[],"lastModifiedDate":"2022-10-17T15:26:53.171278","indexId":"ofr85648E","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1987","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":330,"text":"Open-File Report","code":"OFR","onlineIssn":"2331-1258","printIssn":"0196-1497","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"85-648","chapter":"E","title":"Data on ground-water quality for the McDermitt 1° x 2° quadrangle, northern Nevada","docAbstract":"<p>Water quality data for groundwater were compiled for the McDermitt 1° x 2° quadrangle which covers a portion of northern Nevada. Chemical characteristics of the water are shown on a map (at a scale of 1:250,000) and on trilinear diagrams for the major ions. The data for the area are also presented in a table.&nbsp;</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr85648E","usgsCitation":"Welch, A., and Williams, R.P., 1987, Data on ground-water quality for the McDermitt 1° x 2° quadrangle, northern Nevada: U.S. Geological Survey Open-File Report 85-648, 2 Plates: 40.17 × 24.24 inches and 33.25 × 19.82 inches, https://doi.org/10.3133/ofr85648E.","productDescription":"2 Plates: 40.17 × 24.24 inches and 33.25 × 19.82 inches","costCenters":[],"links":[{"id":165427,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":67962,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1985/0648e/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":67963,"rank":401,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1985/0648e/plate-2.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":392477,"rank":4,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_16875.htm"}],"country":"United States","state":"Nevada","otherGeospatial":"McDermitt 1° x 2° quadrangle","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -118,\n              41\n            ],\n            [\n              -116,\n              41\n            ],\n            [\n              -116,\n              42\n            ],\n            [\n              -118,\n              42\n            ],\n            [\n              -118,\n              41\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b24e4b07f02db6ae409","contributors":{"authors":[{"text":"Welch, Alan H.","contributorId":45286,"corporation":false,"usgs":true,"family":"Welch","given":"Alan H.","affiliations":[],"preferred":false,"id":222898,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Williams, Rhea P.","contributorId":87114,"corporation":false,"usgs":true,"family":"Williams","given":"Rhea","email":"","middleInitial":"P.","affiliations":[],"preferred":false,"id":222899,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":14753,"text":"ofr87571 - 1987 - Regional study of the Castle Hayne Aquifer of eastern North Carolina","interactions":[],"lastModifiedDate":"2016-12-15T13:20:46","indexId":"ofr87571","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1987","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":330,"text":"Open-File Report","code":"OFR","onlineIssn":"2331-1258","printIssn":"0196-1497","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"87-571","title":"Regional study of the Castle Hayne Aquifer of eastern North Carolina","docAbstract":"The Castle Hayne aquifer is an eastward sloping and thickening wedge of limestone and sandstone, located in a 12,500 sq mi area in the eastern part of North Carolina. The Castle Hayne aquifer is the major source of freshwater for much of coastal North Carolina where the aquifers underlying the Castle Hayne contain saltwater. A regional study of the Castle Hayne aquifer was conducted to provide definitive information on the declines in water levels and of saltwater intrusion in the area. A series of geohydrologic maps produced from the study, show the altitude of the top of the aquifer, location of saltwater in the aquifer, aquifer thickness, aquifer transmissivity, and confining-unit thickness. The history of groundwater pumpage can be compared with historical water levels in the aquifer. These geohydrologic, pumpage, and water level data can be used to develop estimates of aquifer and confining-unit hydraulic coefficients and to develop a groundwater flow model for the Castle Hayne aquifer. The model will increase the understanding of the groundwater flow system and also can be used to assess various groundwater development scenarios for the entire Castle Hayne aquifer.","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/ofr87571","usgsCitation":"Lyke, W., and Coble, R.W., 1987, Regional study of the Castle Hayne Aquifer of eastern North Carolina: U.S. Geological Survey Open-File Report 87-571, 2 p. :maps ;28 cm., https://doi.org/10.3133/ofr87571.","productDescription":"2 p. :maps ;28 cm.","costCenters":[{"id":13634,"text":"South Atlantic Water Science Center","active":true,"usgs":true}],"links":[{"id":43523,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1987/0571/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":148696,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1987/0571/report-thumb.jpg"}],"country":"United States","state":"North Carolina","otherGeospatial":"Castle Hayne Aquifer","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -79.03564453124999,\n              33.65120829920497\n            ],\n            [\n              -79.03564453124999,\n              36.633162095586556\n            ],\n            [\n              -74.66308593749999,\n              36.633162095586556\n            ],\n            [\n              -74.66308593749999,\n              33.65120829920497\n            ],\n            [\n              -79.03564453124999,\n              33.65120829920497\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ac9e4b07f02db67c447","contributors":{"authors":[{"text":"Lyke, W.L.","contributorId":75551,"corporation":false,"usgs":true,"family":"Lyke","given":"W.L.","affiliations":[],"preferred":false,"id":169950,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Coble, R. W.","contributorId":49380,"corporation":false,"usgs":true,"family":"Coble","given":"R.","email":"","middleInitial":"W.","affiliations":[],"preferred":false,"id":169949,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":41178,"text":"ofr8734 - 1987 - Potentiometric surface of the upper Floridan aquifer in central Sumter County, Florida, September 1986","interactions":[],"lastModifiedDate":"2022-08-16T20:56:43.038874","indexId":"ofr8734","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1987","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":330,"text":"Open-File Report","code":"OFR","onlineIssn":"2331-1258","printIssn":"0196-1497","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"87-34","title":"Potentiometric surface of the upper Floridan aquifer in central Sumter County, Florida, September 1986","docAbstract":"<p>This map shows the potentiometric surface of the Upper Floridan aquifer in central Sumter County, Florida, for September 1986. The Upper Floridan aquifer is the principal source of potable water in the area. The focus of the map is in the Jumper Creek Canal area where mine pumpage affects water levels. Water levels rose approximately 2 to 3 feet in the southern part of the study area between May and September but remained stable in the northern part. The potentiometric surface ranged in altitude from more than 90 ft in the southeastern part of the county to less than 40 feet northwest of Lake Panasoffkee in the west-central area.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr8734","usgsCitation":"Bradner, L.A., 1987, Potentiometric surface of the upper Floridan aquifer in central Sumter County, Florida, September 1986: U.S. Geological Survey Open-File Report 87-34, 1 Plate: 29.86 × 33.68 inches, https://doi.org/10.3133/ofr8734.","productDescription":"1 Plate: 29.86 × 33.68 inches","costCenters":[],"links":[{"id":175456,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":79010,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1987/0034/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":405230,"rank":3,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_17123.htm","linkFileType":{"id":5,"text":"html"}}],"country":"United States","state":"Florida","county":"Sumter County","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -82.333,\n              28.5\n            ],\n            [\n              -81.917,\n              28.5\n            ],\n            [\n              -81.917,\n              28.917\n            ],\n            [\n              -82.333,\n              28.917\n            ],\n            [\n              -82.333,\n              28.5\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ad4e4b07f02db682b50","contributors":{"authors":[{"text":"Bradner, L. A.","contributorId":21925,"corporation":false,"usgs":true,"family":"Bradner","given":"L.","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":224611,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":4709,"text":"twri03B6 - 1987 - The principle of superposition and its application in ground-water hydraulics","interactions":[{"subject":{"id":15611,"text":"ofr84459 - 1984 - The principle of superposition and its application in ground-water hydraulics","indexId":"ofr84459","publicationYear":"1984","noYear":false,"title":"The principle of superposition and its application in ground-water hydraulics"},"predicate":"SUPERSEDED_BY","object":{"id":4709,"text":"twri03B6 - 1987 - The principle of superposition and its application in ground-water hydraulics","indexId":"twri03B6","publicationYear":"1987","noYear":false,"title":"The principle of superposition and its application in ground-water hydraulics"},"id":1}],"lastModifiedDate":"2012-02-02T00:05:31","indexId":"twri03B6","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1987","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":336,"text":"Techniques of Water-Resources Investigations","code":"TWRI","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"03-B6","title":"The principle of superposition and its application in ground-water hydraulics","docAbstract":"The principle of superposition, a powerful mathematical technique for analyzing certain types of complex problems in many areas of science and technology, has important applications in ground-water hydraulics and modeling of ground-water systems. The principle of superposition states that problem solutions can be added together to obtain composite solutions. This principle applies to linear systems governed by linear differential equations.\r\nThis report introduces the principle of superposition as it applies to ground-water hydrology and provides background information, discussion, illustrative problems with solutions, and problems to be solved by the reader.","language":"ENGLISH","publisher":"U.S. G.P.O.,","doi":"10.3133/twri03B6","issn":"0565-596X","usgsCitation":"Reilly, T.E., Franke, O.L., and Bennett, G.D., 1987, The principle of superposition and its application in ground-water hydraulics: U.S. Geological Survey Techniques of Water-Resources Investigations 03-B6, viii, 28 p. :ill ;26 cm., https://doi.org/10.3133/twri03B6.","productDescription":"viii, 28 p. :ill ;26 cm.","costCenters":[],"links":[{"id":139155,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":298,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/twri/twri3-b6/","linkFileType":{"id":5,"text":"html"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a71e4b07f02db641cca","contributors":{"authors":[{"text":"Reilly, Thomas E. tereilly@usgs.gov","contributorId":1660,"corporation":false,"usgs":true,"family":"Reilly","given":"Thomas","email":"tereilly@usgs.gov","middleInitial":"E.","affiliations":[{"id":493,"text":"Office of Ground Water","active":true,"usgs":true}],"preferred":true,"id":149656,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Franke, O. Lehn","contributorId":63357,"corporation":false,"usgs":true,"family":"Franke","given":"O.","email":"","middleInitial":"Lehn","affiliations":[],"preferred":false,"id":149658,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Bennett, Gordon D.","contributorId":18740,"corporation":false,"usgs":true,"family":"Bennett","given":"Gordon","email":"","middleInitial":"D.","affiliations":[],"preferred":false,"id":149657,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":14924,"text":"ofr87238 - 1987 - Surface-water-quality assessment of the Yakima River basin, Washington: Project description","interactions":[],"lastModifiedDate":"2021-12-23T21:42:36.124756","indexId":"ofr87238","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1987","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":330,"text":"Open-File Report","code":"OFR","onlineIssn":"2331-1258","printIssn":"0196-1497","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"87-238","title":"Surface-water-quality assessment of the Yakima River basin, Washington: Project description","docAbstract":"In April 1986, the U.S. Geological Survey began the National Water Quality Assessment program to: (1) provide a nationally consistent description of the current status of water quality, (2) define water quality trends that have occurred over recent decades, and (3) relate past and present water quality conditions to relevant natural features, the history of land and water use, and land management and waste management practices. At present (1987), The National Water Quality Assessment program is in a pilot studies phase, in which assessment concepts and approaches are being tested and modified to prepare for possible full implementation of the program. Seven pilot projects (four surface water projects and three groundwater projects) have been started. The Yakima River basin in Washington is one of the pilot surface water project areas. The Yakima River basin drains in area of 6,155 sq mi and contains about 1,900 river mi of perennial streams. Major land use activities include growing and harvesting timber, dryland pasture grazing, intense farming and irrigated agriculture, and urbanization. Water quality issues that result from these land uses include potentially large concentrations of suspended sediment, bacteria, nutrients, pesticides, and trace elements that may affect water used for human consumption, fish propagation and passage, contact recreation, livestock watering, and irrigation. Data will be collected in a nine year cycle. The first three years of the cycle will be a period of concentrated data acquisition and interpretation. For the next six years, sample collection will be done at a much lower level of intensity to document the occurrence of any gross changes in water quality. This nine year cycle would then be repeated. Three types of sampling activities will be used for data acquisition: fixed location station sampling, synoptic sampling, and intensive reach studies. (Lantz-PTT)","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr87238","usgsCitation":"McKenzie, S.W., and Rinella, J.F., 1987, Surface-water-quality assessment of the Yakima River basin, Washington: Project description: U.S. Geological Survey Open-File Report 87-238, Report: v, 35 p.; 1 Plate: 31.11 × 31.65 inches, https://doi.org/10.3133/ofr87238.","productDescription":"Report: v, 35 p.; 1 Plate: 31.11 × 31.65 inches","costCenters":[],"links":[{"id":43737,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1987/0238/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":43738,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1987/0238/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":146296,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1987/0238/report-thumb.jpg"},{"id":393389,"rank":4,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_17169.htm"}],"country":"United States","state":"Washington","otherGeospatial":"Yakima River basin","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -121.524,\n              45.972\n            ],\n            [\n              -119.139,\n              45.972\n            ],\n            [\n              -119.139,\n              47.615\n            ],\n            [\n              -121.524,\n              47.615\n            ],\n            [\n              -121.524,\n              45.972\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ae5e4b07f02db68a4b6","contributors":{"authors":[{"text":"McKenzie, S. W.","contributorId":66240,"corporation":false,"usgs":true,"family":"McKenzie","given":"S.","email":"","middleInitial":"W.","affiliations":[],"preferred":false,"id":170257,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Rinella, J. F.","contributorId":86777,"corporation":false,"usgs":true,"family":"Rinella","given":"J.","email":"","middleInitial":"F.","affiliations":[],"preferred":false,"id":170258,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":50777,"text":"ofr8732 - 1987 - Measuring water levels in wells","interactions":[],"lastModifiedDate":"2012-02-02T00:11:35","indexId":"ofr8732","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1987","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":330,"text":"Open-File Report","code":"OFR","onlineIssn":"2331-1258","printIssn":"0196-1497","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"87-32","title":"Measuring water levels in wells","language":"ENGLISH","doi":"10.3133/ofr8732","usgsCitation":"Bond, W., 1987, Measuring water levels in wells: U.S. Geological Survey Open-File Report 87-32, 22 p.; videotape, https://doi.org/10.3133/ofr8732.","productDescription":"22 p.; videotape","costCenters":[],"links":[{"id":177609,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a29e4b07f02db6117a4","contributors":{"authors":[{"text":"Bond, W.T.","contributorId":16091,"corporation":false,"usgs":true,"family":"Bond","given":"W.T.","email":"","affiliations":[],"preferred":false,"id":242286,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":29017,"text":"wri864355 - 1987 - Selected chemical analyses of water from formations of Mesozoic and Paleozoic age in parts of Oklahoma, northern Texas, and Union County, New Mexico","interactions":[],"lastModifiedDate":"2012-02-02T00:08:53","indexId":"wri864355","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1987","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":342,"text":"Water-Resources Investigations Report","code":"WRI","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"86-4355","title":"Selected chemical analyses of water from formations of Mesozoic and Paleozoic age in parts of Oklahoma, northern Texas, and Union County, New Mexico","docAbstract":"Hydrochemical data were compiled into a data base as part of the Central Midwest Regional Aquifer System Analysis project. The data consist of chemical analyses of water samples collected from wells that are completed in formations of Mesozoic and Paleozoic age. The data base includes data from the National Water Data Storage and Retrieval System, the Petroleum Data System, the National Uranium Resource Evaluation, and selected publications. Chemical analyses were selected for inclusion within the hydrochemical data base if the total concentration of the cations differed from the total 10 percent or less of the total concentration of all ions. Those analyses which lacked the necessary data for an ionic balance were included if the ratios of dissolved-solids concentration to specific conductance were between 0.55 and 0.75. The tabulated chemical analyses, grouped by county, and a statistical summary of the analyses, listed by geologic unit, are presented.","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/wri864355","usgsCitation":"Parkhurst, R., and Christenson, S.C., 1987, Selected chemical analyses of water from formations of Mesozoic and Paleozoic age in parts of Oklahoma, northern Texas, and Union County, New Mexico: U.S. Geological Survey Water-Resources Investigations Report 86-4355, iv, 222 p. :ill., maps ;28 cm., https://doi.org/10.3133/wri864355.","productDescription":"iv, 222 p. :ill., maps ;28 cm.","costCenters":[],"links":[{"id":159515,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1986/4355/report-thumb.jpg"},{"id":57882,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1986/4355/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a08e4b07f02db5fa647","contributors":{"authors":[{"text":"Parkhurst, R.S.","contributorId":73625,"corporation":false,"usgs":true,"family":"Parkhurst","given":"R.S.","email":"","affiliations":[],"preferred":false,"id":200796,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Christenson, S. C.","contributorId":98320,"corporation":false,"usgs":true,"family":"Christenson","given":"S.","email":"","middleInitial":"C.","affiliations":[],"preferred":false,"id":200797,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":3720,"text":"cir987 - 1987 - The use of surface geophysical techniques to detect fractures in bedrock; an annotated bibliography","interactions":[],"lastModifiedDate":"2019-08-08T07:45:14","indexId":"cir987","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1987","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":307,"text":"Circular","code":"CIR","onlineIssn":"2330-5703","printIssn":"1067-084X","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"987","title":"The use of surface geophysical techniques to detect fractures in bedrock; an annotated bibliography","docAbstract":"This annotated bibliography compiles references about the theory and application of surface geophysical techniques to locate fractures or fracture zones within bedrock units. Forty-three publications are referenced, including journal articles, theses, conference proceedings, abstracts, translations, and reports prepared by private contractors and U.S. Government agencies. Thirty-one of the publications are annotated. The remainder are untranslated foreign language articles, which are listed only as bibliographic references. \r\n\r\nMost annotations summarize the location, geologic setting, surface geophysical technique used, and results of a study. A few highly relevant theoretical studies are annotated also. Publications that discuss only the use of borehole geophysical techniques to locate fractures are excluded from this bibliography. Also excluded are highly theoretical works that may have little or no known practical application.","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/cir987","usgsCitation":"Lewis, M.R., and Haeni, F., 1987, The use of surface geophysical techniques to detect fractures in bedrock; an annotated bibliography: U.S. Geological Survey Circular 987, iv, 14 p., https://doi.org/10.3133/cir987.","productDescription":"iv, 14 p.","costCenters":[{"id":493,"text":"Office of Ground Water","active":true,"usgs":true}],"links":[{"id":117972,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/circ/1987/0987/report-thumb.jpg"},{"id":30780,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/circ/1987/0987/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a58e4b07f02db62f5f1","contributors":{"authors":[{"text":"Lewis, Mark R.","contributorId":36920,"corporation":false,"usgs":true,"family":"Lewis","given":"Mark","email":"","middleInitial":"R.","affiliations":[],"preferred":false,"id":147480,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Haeni, F.P.","contributorId":87105,"corporation":false,"usgs":true,"family":"Haeni","given":"F.P.","affiliations":[],"preferred":false,"id":147481,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":13147,"text":"ofr87563 - 1987 - Operation of hydrologic data collection stations by the U.S. Geological Survey in 1987","interactions":[],"lastModifiedDate":"2012-02-02T00:06:48","indexId":"ofr87563","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1987","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":330,"text":"Open-File Report","code":"OFR","onlineIssn":"2331-1258","printIssn":"0196-1497","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"87-563","title":"Operation of hydrologic data collection stations by the U.S. Geological Survey in 1987","docAbstract":"The U.S. Geological Survey operates hydrologic data collection stations nationwide which serve the needs of all levels of government, the private sector, and the general public, for water resources information. During fiscal year 1987, surface water discharge was determined at 10,624 stations; stage data on streams, reservoirs, and lakes were recorded at 1,806 stations; and various surface water quality characteristics were determined at 2,901 stations. In addition, groundwater levels were measured at 32,588 stations, and the quality of groundwater was determined at 9,120 stations. Data on sediment were collected daily at 174 stations and on a periodic basis at 878 stations. Information on precipitation quantity was collected at 909 stations, and the quality of precipitation was analyzed at 78 stations. Data collection platforms for satellite telemetry of hydrologic information were used at 2,292 Geological Survey stations. Funding for the hydrologic stations was derived, either solely or from a combination, from three major sources - the Geological Survey 's Federal Program appropriation, the Federal-State Cooperative Program, and reimbursements from other Federal agencies. The number of hydrologic stations operated by the Geological Survey declined from fiscal year 1983 to 1987. The number of surface water discharge stations were reduced by 452 stations; surface water quality stations declined by 925 stations; groundwater level stations declined by 1,051 stations; while groundwater quality stations increased by 1,472 stations. (Author 's abstract)","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/ofr87563","usgsCitation":"Condes de la Torre, A., 1987, Operation of hydrologic data collection stations by the U.S. Geological Survey in 1987: U.S. Geological Survey Open-File Report 87-563, vi, 42 p. :ill., maps ;28 cm., https://doi.org/10.3133/ofr87563.","productDescription":"vi, 42 p. :ill., maps ;28 cm.","costCenters":[],"links":[{"id":146046,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1987/0563/report-thumb.jpg"},{"id":41549,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1987/0563/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4af1e4b07f02db6917f1","contributors":{"authors":[{"text":"Condes de la Torre, Alberto","contributorId":73570,"corporation":false,"usgs":true,"family":"Condes de la Torre","given":"Alberto","email":"","affiliations":[],"preferred":false,"id":167312,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":12299,"text":"ofr87751 - 1987 - South Carolina ground-water quality","interactions":[],"lastModifiedDate":"2016-12-15T13:33:27","indexId":"ofr87751","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1987","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":330,"text":"Open-File Report","code":"OFR","onlineIssn":"2331-1258","printIssn":"0196-1497","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"87-751","title":"South Carolina ground-water quality","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/ofr87751","usgsCitation":"Speiran, G., Oldham, R., Duncan, D., and Know, R., 1987, South Carolina ground-water quality: U.S. Geological Survey Open-File Report 87-751, iv, 9 p. :ill., maps ;28 cm., https://doi.org/10.3133/ofr87751.","productDescription":"iv, 9 p. :ill., maps ;28 cm.","costCenters":[{"id":13634,"text":"South Atlantic Water Science 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